Trace Metal Retention on Biogenic Manganese Oxide Nanoparticles

Manganese oxides produced by microorganisms are abundant environ- mental nanoparticles whose high retention capacity for toxic trace metals, especially lead, is well established. Until very recently, our knowledge of the molecular-scale structure and reactivity of these biogenic Mn4+ oxide minerals was inferred from studies of synthetic analogues pre- pared in the laboratory. However, biogenic Mn oxides and their reactions with trace metals now can be investigated directly using X-ray absorption spectroscopy, thus bringing new insights into the molecular mechanisms behind the very high scavenging efficiency of these minerals. This new knowledge has important implications for the remediation of trace metal contamination.

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December 2025 --The Variscan Orogeny in Europe – Understanding Supercontinent Formation

The Variscan orogen formed between 380 and 300 million years ago through several accretionary and collisional cycles, culminating with the construction of the Pangea supercontinent. This process occurred via sequential opening and closure of oceanic basins, synchronous detachment of Gondwana derived continental ribbons, and their outboard amalgamation onto the Laurussia margin. The Variscan orogen is rather unique compared with other orogenic belts on Earth: its overthickened and dominantly magmatic crust in the central belt, surprisingly minor mantle involvement in the magmatic and geodynamic processes, coherent and pulsed magmatism along the collision suture, and its complex accretionary history. Because its final product, Pangea, is the youngest and best-understood supercontinent on Earth, the Variscan orogeny offers clues for understanding the mechanisms of supercontinent formation.